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Salinity effect on trace element incorporation in cultured shells of the large benthic foraminifer Operculina ammonoides

Salinity effect on trace element incorporation in cultured shells of the large benthic foraminifer Operculina ammonoides
Salinity effect on trace element incorporation in cultured shells of the large benthic foraminifer Operculina ammonoides
The ratio of sodium to calcium in the shells of foraminifera (Na/Cashell) has been experimentally calibrated as a proxy for past ocean Ca concentrations (Hauzer et al., 2018, https://doi.org/10.1016/j.epsl.2018.06.004). In parallel, it has been suggested that Na/Cashell could be used as a proxy for paleo-salinity. In this study, we determined the extent to which foraminiferal Na/Ca (and other elements) change with salinity for the shallow-dwelling large benthic foraminifer Operculina ammonoides, an extant relative of the abundant Eocene Nummulites. The culture experiment was conducted under four salinities between 33 and 43 psu. Shell chemistry was measured by LA-ICPMS with the newly precipitated CaCO3 identified by a 135Ba-spike added to the experimental seawater. Na/Cashell, Mg/Cashell and Li/Cashell in O. ammonoides increased slightly with salinity, while Sr/Cashell showed no resolvable change. The change in Na/Cashell due to salinity was small (∼1.4%/psu) compared to the changes in this ratio caused by varying seawater calcium concentrations (Casw) with a sensitivity of ∼5%/(mmol kg−1) Casw. Moreover, the change in salinity in most regions of the past open oceans is minor compared to the large secular variations in Casw during the Phanerozoic (10–40 mmol kg−1). Thus, if at all, paleo-salinity may be reconstructed based on Na/Cashell only for samples younger than Casw residence time (∼1 Myr). Furthermore, both regional and global changes in ocean salinity over geological time do not pose a significant complication for the use of Na/Cashell as a proxy for past changes in seawater calcium concentrations.
2572-4525
Hauzer, Hagar
68d86aec-9d2c-4c71-9b63-0fedac4ed501
Evans, David
878c65c7-eab9-4362-896b-166e165eb94b
Müller, Wolfgang
360a71f7-0b47-4ff3-8c32-1912d70401aa
Rosenthal, Yair
0130f66f-7653-490b-b323-76956e66c9e1
Erez, Jonathan
ed56a557-377e-4b63-8ba8-3d23e506e5c0
Hauzer, Hagar
68d86aec-9d2c-4c71-9b63-0fedac4ed501
Evans, David
878c65c7-eab9-4362-896b-166e165eb94b
Müller, Wolfgang
360a71f7-0b47-4ff3-8c32-1912d70401aa
Rosenthal, Yair
0130f66f-7653-490b-b323-76956e66c9e1
Erez, Jonathan
ed56a557-377e-4b63-8ba8-3d23e506e5c0

Hauzer, Hagar, Evans, David, Müller, Wolfgang, Rosenthal, Yair and Erez, Jonathan (2021) Salinity effect on trace element incorporation in cultured shells of the large benthic foraminifer Operculina ammonoides. Paleoceanography and Paleoclimatology, [e2021PA004218]. (doi:10.1029/2021PA004218).

Record type: Article

Abstract

The ratio of sodium to calcium in the shells of foraminifera (Na/Cashell) has been experimentally calibrated as a proxy for past ocean Ca concentrations (Hauzer et al., 2018, https://doi.org/10.1016/j.epsl.2018.06.004). In parallel, it has been suggested that Na/Cashell could be used as a proxy for paleo-salinity. In this study, we determined the extent to which foraminiferal Na/Ca (and other elements) change with salinity for the shallow-dwelling large benthic foraminifer Operculina ammonoides, an extant relative of the abundant Eocene Nummulites. The culture experiment was conducted under four salinities between 33 and 43 psu. Shell chemistry was measured by LA-ICPMS with the newly precipitated CaCO3 identified by a 135Ba-spike added to the experimental seawater. Na/Cashell, Mg/Cashell and Li/Cashell in O. ammonoides increased slightly with salinity, while Sr/Cashell showed no resolvable change. The change in Na/Cashell due to salinity was small (∼1.4%/psu) compared to the changes in this ratio caused by varying seawater calcium concentrations (Casw) with a sensitivity of ∼5%/(mmol kg−1) Casw. Moreover, the change in salinity in most regions of the past open oceans is minor compared to the large secular variations in Casw during the Phanerozoic (10–40 mmol kg−1). Thus, if at all, paleo-salinity may be reconstructed based on Na/Cashell only for samples younger than Casw residence time (∼1 Myr). Furthermore, both regional and global changes in ocean salinity over geological time do not pose a significant complication for the use of Na/Cashell as a proxy for past changes in seawater calcium concentrations.

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More information

Accepted/In Press date: 28 May 2021
e-pub ahead of print date: 7 June 2021
Published date: 23 June 2021

Identifiers

Local EPrints ID: 502585
URI: http://eprints.soton.ac.uk/id/eprint/502585
ISSN: 2572-4525
PURE UUID: 6f9740b4-ed44-44fd-8437-ab0b22ee2af9
ORCID for David Evans: ORCID iD orcid.org/0000-0002-8685-671X

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Date deposited: 01 Jul 2025 16:41
Last modified: 03 Jul 2025 02:36

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Contributors

Author: Hagar Hauzer
Author: David Evans ORCID iD
Author: Wolfgang Müller
Author: Yair Rosenthal
Author: Jonathan Erez

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